AndersonMO.2013. A geological, geochemical and textural study of an LCT pegmatite: implications for the magmatic versus metasomatic origin of Nb-Ta mineralization in the Moose II pegmatite, Northwest territories, Canada.J Geosci. 58:299–320. doi: 10.3190/jgeosci.149
2.
BadaninaEV, 2015. Mineral chemistry of columbite–tantalite from spodumene pegmatites of Kolmozero, Kola Peninsula (Russia).Ore Geo Rev. 64:720–735. doi: 10.1016/j.oregeorev.2014.05.009
3.
BarrosR, MenugeJF.2016. The origin of spodumene pegmatites associated with the Leinster granite In Southeast Ireland.Can Min. 54:847–862. doi: 10.3749/canmin.1600027
4.
DewaeleS, 2011. Late neoproterozoic overprinting of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa).J Afr Earth Sci. 61:10–26. doi: 10.1016/j.jafrearsci.2011.04.004
5.
KaeterD, 2018. The magmatic–hydrothermal transition in rare-element pegmatites from southeast Ireland: LA-ICP-MS chemical mapping of muscovite and columbite–tantalite.Geochim Cosmochim Ac. 240:98–138. doi: 10.1016/j.gca.2018.08.024
6.
LinnenLR, CuneyM.2005. Granite-related rare-element deposits and experimental constrains on Ta-Nb-W-Sb-Zr-Hf mineralization. In: LinnenLR, SamsonIM, editors. Rare-element geochemistry and mineral deposits. GAC Short Course Notes 17. St. Catharines (ON): Geological Association of Canada; p. 48–68.